USE OF THE REVISED UNIVERSAL SOIL LOSS EQUATION AND GIS TECHNIQUES TO MODEL SOIL EROSION RISK IN ROCKY MOUNTAIN NATIONAL PARK

Janke J and Mallory D. 2010. USE OF THE REVISED UNIVERSAL SOIL LOSS EQUATION AND GIS TECHNIQUES TO MODEL SOIL EROSION RISK IN ROCKY MOUNTAIN NATIONAL PARK

The Revised Universal Soil Loss Equation (RUSLE) was used in conjunction with GIS raster modeling techniques to estimate potential soil erosion in Rocky Mountain National Park (ROMO). Currently, 6% of ROMO consists of soils with erosion rates greater than 5 tons/acre/year. The following regions have high erosion rates: 1) east of Long’s Peak; 2) along Stormy Peaks Pass Trail; 3) along the Continental Divide near the southern edge of the Park’s boundary; and 4) in the Hayden Lake area. Jim’s Grove Trail, the Alluvial Fan Trail, East Long’s Peak Trail, and Stormy Peaks Pass Trail have more than 30% of their extent underlain by highly erosive soils. Simulations were run to determine the effects of increased tree mortality from pine beetle kill on soil erosion rates. According to the post-pine beetle model, erosion rates greater than 5 tons/acre/year cover 33% of ROMO, a 28% increase from previous categorized high erosion areas. Bowen-Baker Gulch, Twin-Gem, Bear Lake Bypass, and Bierstadt Mountain Trails have more than 90% of their length underlain by highly erosive soils following the pine beetle disturbance. If a fire were to occur, soil erosion could enhance the frequency of debris flows and slides, especially during short, intense precipitation events. The methods employed in this study only identify high-risk areas of erosion, a useful management tool for narrowing sites from a larger geographic region; however, actual erosion rates should be verified in the field.

Type
Unpublished Report
Authors
Janke, Jason; Mallory, Dwight
Date of Issue
2010
Units
ROMO

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